Structure Functions and Spectra of Scalar Quantities in the Inertial–Convective and Viscous–Convective Ranges of TurbulenceSource: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 014::page 2245Author:Hill, Reginald J.
DOI: 10.1175/1520-0469(1989)046<2245:SFASOS>2.0.CO;2Publisher: American Meteorological Society
Abstract: The Obukhov?Corrsin constants (often referred to as Kolmogorov constants) are the constants of proportionality in formulas pertaining to the inertial-convective range of structure functions (or spectra) of scalar quantities and the cross-structure functions (or cospectra) of pairs of scalar quantities. These Obukhov?Corrsin constants are shown to be equal for all scalar quantities and pairs of scalar quantities. The inertial-convective and viscous-convective range formulas for cross-structure functions (or cospectra) can be deduced from those of the structure functions (or spectra). Special attention is given to the case of dimensionless scalar quantities like refractive index for which the inertial-convective and viscous-convective range formulas can be deduced by several different arguments. Dimensional analysis is useful for the structure functions, cross-structure functions, spectra and cospectra of the inertial-convective range and for the spectra and cospectra in the viscous-convective range. The structure and cross-structure functions do not possess viscous-convective ranges distinct from their viscous-diffusive ranges, however, and dimensional analysis gives incorrect results in this case.
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| contributor author | Hill, Reginald J. | |
| date accessioned | 2017-06-09T14:29:09Z | |
| date available | 2017-06-09T14:29:09Z | |
| date copyright | 1989/07/01 | |
| date issued | 1988 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-20137.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4156332 | |
| description abstract | The Obukhov?Corrsin constants (often referred to as Kolmogorov constants) are the constants of proportionality in formulas pertaining to the inertial-convective range of structure functions (or spectra) of scalar quantities and the cross-structure functions (or cospectra) of pairs of scalar quantities. These Obukhov?Corrsin constants are shown to be equal for all scalar quantities and pairs of scalar quantities. The inertial-convective and viscous-convective range formulas for cross-structure functions (or cospectra) can be deduced from those of the structure functions (or spectra). Special attention is given to the case of dimensionless scalar quantities like refractive index for which the inertial-convective and viscous-convective range formulas can be deduced by several different arguments. Dimensional analysis is useful for the structure functions, cross-structure functions, spectra and cospectra of the inertial-convective range and for the spectra and cospectra in the viscous-convective range. The structure and cross-structure functions do not possess viscous-convective ranges distinct from their viscous-diffusive ranges, however, and dimensional analysis gives incorrect results in this case. | |
| publisher | American Meteorological Society | |
| title | Structure Functions and Spectra of Scalar Quantities in the Inertial–Convective and Viscous–Convective Ranges of Turbulence | |
| type | Journal Paper | |
| journal volume | 46 | |
| journal issue | 14 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1989)046<2245:SFASOS>2.0.CO;2 | |
| journal fristpage | 2245 | |
| journal lastpage | 2251 | |
| tree | Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 014 | |
| contenttype | Fulltext |